Deducing Mineralogy of Serpentinized and Carbonated Ultramafic Rocks Using Physical Properties With Implications for Carbon Sequestration and Subduction Zone Dynamics-Reference-Cited by-同舟云学术

Deducing Mineralogy of Serpentinized and Carbonated Ultramafic Rocks Using Physical Properties With Implications for Carbon Sequestration and Subduction Zone Dynamics

Published:2021-09 Issue:9 Volume:22 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem Geophys Geosyst

Author:

Cutts J. A.¹^ORCID,Steinthorsdottir K.¹^ORCID,Turvey C.¹^ORCID,Dipple G. M.¹^ORCID,Enkin R. J.²^ORCID,Peacock S. M.¹^ORCID

Affiliation:

1. Department of Earth, Ocean and Atmospheric Sciences CarbMin Lab The University of British Columbia Vancouver BC Canada

2. Geological Survey of Canada‐Pacific Sidney BC Canada

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GC009989

Reference98 articles.

1. Unraveling the sequence of serpentinization reactions: petrography, mineral chemistry, and petrophysics of serpentinites from MAR 15°N (ODP Leg 209, Site 1274)

2. Seawater‐peridotite interactions: First insights from ODP Leg 209, MAR 15 N;Back W.;Geochemistry, Geophysics, Geosystems,2004

3. Onset and Progression of Serpentinization and Magnetite Formation in Olivine-rich Troctolite from IODP Hole U1309D

4. Metamorphism of deep-seated rocks from the Garrett Ultrafast Transform (East Pacific Rise near 13°25′S)

5. Magnetic properties, opaque mineralogy and magnetic anisotropies of serpentinized peridotites from ODP Hole 670A near the Mid-Atlantic Ridge

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